SREL Reprint #2744

 

 

 

Response to Comment on "Otolith δ18O Record of Mid-Holocene Sea Surface Temperatures in Peru"

C. Fred T. Andrus1, Douglas E. Crowe2, Daniel H. Sandweiss3, Elizabeth J. Reitz4,
Christopher S. Romanek1,2, and Kirk A. Maasch5

1Savannah River Ecology Laboratory, University of Georgia, Drawer E, Aiken, SC 29802, USA
2Department of Geology, University of Georgia, Athens, GA 30602, USA
3Department of Anthropology and Institute for Quaternary and Climate Studies, S. Stevens Hall,
University of Maine, Orono, ME 04469, USA
4Department of Anthropology and Georgia Museum of Natural History, Natural History Building,
University of Georgia, Athens, GA 30602, USA
5Department of Earth Sciences and Institute for Quaternary and Climate Studies,
University of Maine, Bryand Global Sciences Center, Orono, ME 04469, USA

Introduction: We find arguments of Béarez et al. unconvincing. We did not contend that Galeichtys peruvianus is a topical species. Rather, G. peruvianus was selected for its wide temperature tolerance and was captured during both El Niño and La Niña events in Huanchaco, Peru. The northern range boundary Béarez et al cite (6°S) is incorrect. In a prior publication Béarez stated that this species is native to Ecuador, an observation corroborated by other authors, which undermines the cool climate suggestion. Our sea surface temperature (SST) conclusions rely on δ18O data, not the presence or absence of species [although presence-absence data show predominantly tropical fauna at Ostra and Siches]. . .

SREL Reprint #2744

Andrus, C. F. T., D. E. Crowe, D. H. Sandweiss, E. J. Reitz, and C. S. Romanek. 2003. Response to comment on "Otolith δ18O record of mid-holocene sea surface temperatures in Peru". Science 299:203b.

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